View Original Image at Full SizeThe Carrabassett Formation is comprised of pelitic turbidites and olistostromes (mostly slump and debris flows) deposited in an actively migrating foredeep during the Acadian Orogeny.
Image 12340 is a 317 by 700 pixel WebP
Uploaded:
Jul14 08
Permanent URL: https://serc.carleton.edu/download/images/12340/sedimentary_model_carrabassett.webp
The file is referred to in 1 page
Provenance
Image by Lindley Hanson.
ReuseThis item is offered under a Creative Commons Attribution-NonCommercial-ShareAlike license
http://creativecommons.org/licenses/by-nc-sa/3.0/ You may reuse this item for non-commercial purposes as long as you provide attribution and offer any derivative works under a similar license.